Variscan Sn-W-Mo metallogeny in the gravity picture of the Krusne hory/Erzgebirge granite batholith (Central Europe)

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10296062" target="_blank" >RIV/00216208:11310/15:10296062 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.oregeorev.2015.02.014" target="_blank" >http://dx.doi.org/10.1016/j.oregeorev.2015.02.014</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.oregeorev.2015.02.014" target="_blank" >10.1016/j.oregeorev.2015.02.014</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Variscan Sn-W-Mo metallogeny in the gravity picture of the Krusne hory/Erzgebirge granite batholith (Central Europe)

Popis výsledku v původním jazyce

Late Variscan wolframite (+/- molybdenite) and cassiterite-wolframite greisen, skarn and vein deposits occur in a close spatial association with the granites of the Krusne hory/Erzgebirge batholith (KHEB) in Central Europe. We examined the distribution of the deposits in relation to the gravity field affected by Late Variscan granites using the data from previous gravity and metallogenic studies. Late Variscan granites are differentiated into earlier biotite monzogranites (low-F granites) and later biotite or lithium mica syenogranites (high-F granites) in accordance with the previous classifications. All the outcrops of granites in the KHEB region and their hidden continuation are confined to the Bouguer anomaly contour of 20 mGal. The Sn-W-Mo (rare metal) deposits and occurrences are within the gravity contour of 30 mGal with the exception of the Grossschirma stratiform tin deposit in the Freiberg polymetallic ore district. We constructed a geological model based on the gravity data

Název v anglickém jazyce

Variscan Sn-W-Mo metallogeny in the gravity picture of the Krusne hory/Erzgebirge granite batholith (Central Europe)

Popis výsledku anglicky

Late Variscan wolframite (+/- molybdenite) and cassiterite-wolframite greisen, skarn and vein deposits occur in a close spatial association with the granites of the Krusne hory/Erzgebirge batholith (KHEB) in Central Europe. We examined the distribution of the deposits in relation to the gravity field affected by Late Variscan granites using the data from previous gravity and metallogenic studies. Late Variscan granites are differentiated into earlier biotite monzogranites (low-F granites) and later biotite or lithium mica syenogranites (high-F granites) in accordance with the previous classifications. All the outcrops of granites in the KHEB region and their hidden continuation are confined to the Bouguer anomaly contour of 20 mGal. The Sn-W-Mo (rare metal) deposits and occurrences are within the gravity contour of 30 mGal with the exception of the Grossschirma stratiform tin deposit in the Freiberg polymetallic ore district. We constructed a geological model based on the gravity data

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

—

Projekt

—

Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Ore Geology Reviews

ISSN

0169-1368

e-ISSN

—

Svazek periodika

69

Číslo periodika v rámci svazku

Sep

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

16

Strana od-do

285-300

Kód UT WoS článku

000356754500017

EID výsledku v databázi Scopus

2-s2.0-84929756262